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Metamorphism-facilitated faulting in deforming orthopyroxene: Implications for global intermediate-depth seismicity
Intermediate-depth earthquakes that occur between ∼60- and 300-km depths in subducted oceanic slabs often form a double band of seismicity. The upper band of seismicity is predominantly within the basaltic crust and is thought to be facilitated by processes related to dehydration reactions. More con...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
National Academy of Sciences
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8931219/ https://www.ncbi.nlm.nih.gov/pubmed/35254914 http://dx.doi.org/10.1073/pnas.2112386119 |